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Ecology
scientific study of the interactions between organisms and the environment
reveals the richness of the biosphere
these interactions determine distribution of organisms and their abundance
derived from the words
oikos (home)
logos (study)
types of ecology
global ecology
landscape ecology
ecosystem evology
community ecology
population ecology
organismal ecology
organismal ecology
studies how an organism’s structure, physiology, and behaviour meet environmental challenges
population
group of individuals of the same species living in an area
population ecology
focuses on factors affecting how many individuals of a species live in an area
community
group of populations of different species in an area
community ecology
deals with the whole array of interacting species in a community
ecosystem
community of organisms in an area and the physical factors where they interact
ecosystem ecology
emphasizes energy flow and chemical cycling among various biotic and abiotic componenets
landscape
mosaic of connected ecosystems
landscape ecology
deals with arrays of ecosystems and how they are arranged in a geographic region
biosphere
global ecosystem
sum of all the planet’s ecosystens
global ecology
examines the influence of energy and materials on organisms across the biosphere
regional effects on climate
Seasonality
in middle to high latitudes, Earth’s tilted axis of rotation and annual passage around the sun cause strong seasonal cycles in day length, solar radiation, and temperature
Bodies of water
ocean currents influence climate along the coasts of continents by heating or cooling overlying air masses that pass across the land
coastal regions are also more wetter than inland regions
Mountains
influence air flow over land
as warm air approaches a mountain, moisture is released on the windward side
biomes
major ecological associations that occupy broad geographic regions of land or water
varying combinations of biotic and abiotic factors determine the nature of biomes
terrestrial biomes are defined by the vegetation type
aquatic biomes are defined by the physical environment
general features of terrestrial biomes
major physical or climatic features and dominant vegetation
vertical layering of vegetation is an important feature of terrestrial biomes
layering of vegetation creates different habitats for animals
Tropical forest Climate
Climate
usually high temp.
rain forests 200-400cm of rain anually
dry forests 150-200cm of rain anually
Tropical Forest Organisms
vertically layered forests and plants compete for light
home to millions of species
animal diversity higher than any other terrestrial biomes layering
Human impact on tropical forests
rapid population growth leading to agriculture and development is destroying many tropical forests
Savanna Climate
Climate
rainfall averages 30-50cm per year and is seasonal
temp averages 24-29*C
Savanna organisms
scattered trees and are often thorny
fires are common in dry season and dominant plant species are fire adapted
grasses and forbs - primary ground cover
large herbivorous mammals and their predators are common
human impact on Savanna
frequent human-caused fires prevent regeneration
cattle ranching and overhunting reduces large mammal populations
Desert climate
Climate
low precipitation - less than 30cm of rain per year
temp. varies seasonally and daily
> 50*C in hot desserts
< 30*C in colds desserts
Desert organisms
dominated by low, widely scattered vegetation
plant adaptations include tolerance to heat and desiccation, water storage, reduced leaf area, and physical defences against herbivores
human impact on desert
long distance water transport and deep wells have allowed humans to live in desserts
urbanization and agriculture have reduced biodiversity
Chaparral climate
Climate
30-50cm annual precipitation
rainy winters, dry summers
Chaparral organisms
shrubs - small trees that are fire adapted
some germinate only after fires
adapted to droyght
animals: browsers like deers and goats, insects, small mammals, amphibians, birds
human impact on chaparral
have been heavily settled and reduced through conversion to agriculture and urbanization
Humans contribute to fires
Temperate grassland climate
climate
annual precipitation 30-100cm
dry winters, wet summers
temperate grassland organisms
dominated by grasses and forbs
plants adapted to drought, fire
grazing by animals (bison and wild horses) prevents establish of trees
burrowing animals are common
human impact on temperate grasslands
many grasslands have been converted to farm and grazing lands
grazing has converted some dry grassland to desert
Northern coniferous forest climate
Climate
annual precipitation 30-70cm
cold winters
large annual temp. range
Northern coniferous forest organisms
conifers are common
some depend on fire to regenerate
plant diversity lower than broadleaf forests
Mammals: moose, brown bears, siberian tigers
insect outbreaks can kill trees
human impact on Northern coniferous forest
northern forests are logged at a fast rate
old growth forests are under threat
temperate broadleaf forest climate
annual precip. 70-200cm
winter low about 0*C, humid summers max 35*C
temperate broadleaf forest organisms
dominant plants are deciduous trees
in Australia, evergreen eucalyptus trees are common
northern hemisphere, many mammals hibernate and birds migrate south
human impact on temperate broadleaf forests
have been heavily settled, and destroyed by logging and land clearing
Tundra climate
annual precip. 20-60cm in arctic tundra
up to 100cm in alpina tundra
cold winters, summer max 10*C
tundra organisms
vegetation mostly herbaceous
mosses, grasses, and forbs
permafrost restricts growth of plant roots
musk oxen live here
migratory caribou
predators: bears, wolves, foxes, and snowy owls
human impact on tundra
sparsely settled
mineral and oil extraction in some areas
Division of aquatic biomes
see image

Wetlands and estuaries physical environment
Physical environment
inundated by water at least some of year
estuary a transition between river and sea
highly productive habitats
wetlands and estuaries organisms
water saturated soils favour growth of plants like cattails and sedges
herbivores: crustaceans, aquatic insect larvae, muskrats
predators: dragonflies, frogs, alligators, herons
estuaries support oysters, crabs, fish
human impact on wetlands and estuaries
drainage widespread
filling, dredging, pollution disrupt estuaries
Lakes physical environment
light decreases with depth
seasonal lakes may have thermocline
eutrophic lakes are nutrient rich
lake organisms
rooted and floating aquatic plants in littoral zone
phytoplankton in limnetic zone
zooplankto grazers
invertabrates in benthic zone
fish in all zones with sufficien oxygen
human impact on lakes
runoff from fertilized lands leads to eutropication
wetland
habitat that is inundated by water at least some of the time and supports plants adapted to water-saturated soil
can develop in shallow basins, along flooded river banks, or on coasts of large lakes and seas
Prairie pothole region
stretches across southern prairies
750,000 cm²
millions of depressions fill with snow melt and rain
why are wetlands good
they act like giant sponges
soak up rain and snowmelt and release water in drier season
reduces erosion and flooding and filter water
wetland conservation
2/3 of prairie wetlands are gone
at risk to global warming
one of the most productive biomes on earth
streams and rivers physical environment
headwaters clear and cold
downstream water warmer and more turbid
streams and rivers organisms
headwaters may be rich in phytoplankton or rooted aquatic plants
diverse fishes and invertebrates inhabit unpolluted streams and rivers
human impact on streams and rivers
municipal, agricultural, and industrial pollution degrade water quality
dams impair natural flow of streams and rivers
intertidal zones physical environment
periodically submerged by tides twice daily
upper strata experience more exposure to air and greater variations in temp. and salinity
intertidal zones organisms
diverse marine algae
sandy zones lack attached plants or algae
some animals adapted to attaching to rocks
many animals in sandy or muddy areas bury themselves and feed on riding tides
human impact on intertidal zones
oil pollution has disrupted many intertidal communities
coral reefs physical environment
physical environment
formed largely from calcium carbonate skeletons of corals
shallow reef building corals live in clear photic zone of tropical seas
coral reefs organisms
unicellular algae live within tissues of corals in mutualism
provides coral with organic molcules
high density of fish invertebrate in corals
species diversity rivals tropical forests
human impact on coral reefs
global warming and pollution contribute to large-scale coral death
oceanic pelagic zone physical environment
physical environment
vast realm of open blue water
surface constantly mixed by wind-driven currents
covers 70% of earth
ocean pelagic zone organisms
dominant photosynthetic organisms - bacteria and other phytoplankton
account for half of global productivity
zooplankton eat phytoplankton
free-swimming animals: squid, fish, sea turtles, sea mammals
human impact on ocean pelagic zone
overfishing has depleted fish stocks
oceans affected by climate warming and pollution
marine benthic zone
sea floor
temp declines and pressure increases with depth
marine benthic zone organisms
seaweeds live in shallow benthic areas
prokaryotes - food producers in deep sea vents
coastal benthic communities - invertebrates and fishes
human impact on marine benthic zone
overfishing has depleted benthic fish populations
dumping of organic wastes creates anoxia
what limits the distribution of species
interactions between organisms and the environment
affect of dispersal on distrbution
can limit distribution due to area inaccessible or insufficient time

affect of biotic factors on distribution of species
predation, parasitism, competition, disease

affect of abiotic factors on distribution of species
physical factors - temp., light, soil structure, fire, moisture, etc.
chemical factors - water, oxygen, sainity, pH, soil nutrients, etc.
dispersal
the movement of individuals away from centers of high population density or from their area of origin
contributes to global distribution of organisms
natural range expansions show influence of disperson on distribution
ex. cattle egret
species transplants
organisms that are intentionally or accidentally relocated from their original distribution
can disrupt the communities or ecosystems they are introduced to
biotic factors that affect distribution of organisms
interactions with other species
predation
competition
Abiotic factors affecting distribution
temp.
water and oxygen
salinity
sunlight
rocks and soil
affect of temp. on distribution of organisms
important factor due to its effects on biological processes
cells may freeze and rupture below 0*C
most proteins denature above 45*C
mammals and birds use up energy to regulate internal temp.
water and oxygen affect on distribution of organisms
water availability
ex. desert organism adaptations for water conservation
salinity effect on distribution of organisms
salt concentration affects water balance of organisms through osmosis
few terrestrial organisms are adapted to high-salinity habitats
sunlight affect on distribution of organisms
light intensity and quality affect photosynthesis
water absorbs light causing most photosynthesis to occur near the surface of aquatic environments
in deserts, high light levels increase temp. and can stress plants and animals
rocks and soils affect on distribution of organisms
many characteristics of soil limit distribution of plants and the animals that eat them
physical structure
pH
mineral composition